Solid-state C-13 NMR analysis of size and density fractions of marine sediments: Insight into organic carbon sources and preservation mechanisms
Date
2006
Authors
Dickens, A.
Baldock, J.
Smernik, R.
Wakeham, S.
Arnarson, T.
Gelinas, Y.
Hedges, J.
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Journal article
Citation
Geochimica et Cosmochimica Acta, 2006; 70(3):666-686
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Angela F. Dickens, Jeffrey A. Baldock, Ronald J. Smernik, Stuart G. Wakeham, Thórarinn S. Arnarson, Yves Gélinas and John I. Hedges
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Abstract
Burial of organic carbon (OC) in ocean sediments acts as the ultimate long-term sink for both terrestrial and marine carbon, however, the mechanisms controlling the preservation of this carbon are poorly understood. To better understand these mechanisms, we applied solid-state <sup>13</sup>C nuclear magnetic resonance (NMR) spectroscopy, along with elemental, stable carbon isotopic (δ<sup>13</sup>C) and lignin phenol analyses, to size and density fractions of sediments influenced by either mixed terrestrial and marine OC inputs (Washington Coast slope) or dominantly marine inputs (Mexican Margin). Elemental, isotopic and lignin analyses all reveal that within the Washington Coast sediment, the OC mixes linearly between nitrogen-poor and <sup>13</sup>C-depleted, lignin-rich OC in the large and light fractions and nitrogen-rich and <sup>13</sup>C-enriched, lignin-poor OC in the small and dense fractions, suggesting that this sediment contains a two-component mixture of terrestrial vascular plant- and marine-derived OC. The integral areas of each of seven NMR spectral regions in the different samples trend linearly when plotted versus δ<sup>13</sup>C signature, with most R<sup>2</sup> values of 0.78 or greater, demonstrating that the NMR spectra of the two sources of carbon also mix linearly between the two endmembers. The terrestrial endmember in this sediment appears to be dominated by lignin and black carbon whereas the source of the marine endmember is less clear from the NMR spectra. In contrast, all of the analyses indicate that OC in the Mexican Margin sediment fractions is homogenous and derives almost exclusively from marine sources. It appears that selective preservation of (bio)chemically recalcitrant lignin and black carbon is the primary mechanism of preservation of terrestrial OC, whereas mineral-protection is the dominant mechanism preserving marine OC in the Washington coast sediment. There is little evidence showing that either preservation mechanism functions in the Mexican Margin sediments. © 2005 Elsevier Inc. All rights reserved.
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Copyright © 2005 Elsevier Inc. All rights reserved.